The geological time scale is a system of chronological dating that relates geological strata to time. It is used by geologists, paleontologists, and other Earth scientists to describe the timing and relationships between events that have occurred during the Earth'shistory. The time scale is divided into eons, eras, periods, epochs, and ages, and it provides a framework for understanding the history and evolution of the Earth.
Key Concepts
Eons: The largest division of time on the geological time scale, representing billions of years. The current eon is the Phanerozoic eon, which began around 541 million years ago.
Eras: Eons are subdivided into eras, which are characterized by significant geological and biological events. The Phanerozoic eon is divided into three eras: the Paleozoic, Mesozoic, and Cenozoic eras.
Periods: Eras are further divided into periods, each associated with distinct rock layers and fossil assemblages. For example, the Mesozoic era is divided into the Triassic, Jurassic, and Cretaceous periods.
Epochs: Periods are divided into epochs, which are defined by specific changes in the Earth'senvironment and biota.
Ages: The smallest units of geological time, ages are defined by specific rock layers and the fossils found within them.
Study Guide
When studying the geological time scale, it is important to understand the major eons, eras, and periods, as well as the key events and life forms associated with each. Additionally, familiarizing yourself with the concept of relative and absolute dating methods will help you understand how scientists determine the ages of rocks and fossils.
Key topics to cover include:
The three major eras of the Phanerozoic eon and their defining characteristics
Analyze and interpret data for patterns of change in anatomical structures of organisms using the fossil record and the chronological order of fossil appearance in rock layers.